Enfeng Liu

Biographic Data

ID	3637242
NAME	Enfeng Liu
GIVEN NAMES	Enfeng
FAMILY NAME	Liu
SIGNATURE	LIU E
AFFILIATIONS	Shandong Normal University
VERIFIED	No
TOTAL WORKS	10
TOTAL CITATIONS	7
WORKS AS AUTHOR	10
WORKS AS EDITOR	0
FIRST PUBLICATION YEAR	2014
LATEST PUBLICATION YEAR	2026
H-INDEX	1

Centurial heavy metal enrichment from an alpine lake in southwest China
Open AccessJianing Fan, Yongbo Wang et al.ARTICLEAnthropocene2026
A quantitative temperature reconstruction of the ‘Little Ice Age’ in southern China
Open AccessJie Chang, Enlou Zhang et al.ARTICLEThe Holocene2020References: 4
We present a branched glycerol dialkyl glycerol tetraethers (brGDGTs)–based mean annual temperature reconstruction covering the last millennium from a subtropical lake in Guangxi Province, southern China (23°N). We demonstrate that the pattern and absolute values of mean annual temperatures reconstructed using the eastern African lake brGDGTs calibration based on the methylation of 5-methyl branched tetraethers index provided the most reliable an…
Deciphering centurial anthropogenic pollution processes in large lakes dominated by socio-economic impacts
Open AccessQi Lin, Ke Zhang et al.ARTICLEAnthropocene2020References: 65
Geochemistry of the holocene sediments of Lake Chenghai, SW China, and its implications for paleoenvironmental reconstruction
Open AccessWeiwei Sun, Enfeng Liu et al.ARTICLEQuaternary International2019
A lacustrine record of East Asian summer monsoon and atmospheric dust loading since the last interglaciation from Lake Xingkai, northeast China
Open AccessWeiwei Sun, Ji Shen et al.ARTICLEQuaternary Research2018
A 336-cm-long sediment core spanning the last 130 ka was recovered from Lake Xingkai on the northeastern margin of the East Asian summer monsoon domain to reveal the linkage between lacustrine depositional processes and environmental changes. Bayesian end member modeling analysis was conducted to partition and interpret the grain-size distributions of Lake Xingkai sediments. Our results suggest that the sedimentary system is characterized by thre…
A 60-year historical record of polycyclic aromatic hydrocarbons (PAHs) pollution in lake sediment from Guangxi Province, Southern China
Open AccessJie Chang, Enlou Zhang et al.ARTICLEAnthropocene2018
Summer temperature variability inferred from subfossil chironomid assemblages from the south-east margin of the Qinghai–Tibetan Plateau for the last 5000 years
Open AccessJie Chang, Enlou Zhang et al.ARTICLEThe Holocene2017Cited by: 1References: 16
We present a quantitative mean July temperature record spanning the last c. 5000 years from an alpine lake in south-western China. The reconstruction is based on the application of an established chironomid-based inference model using 100 lakes from the region. The reconstructed summer temperature changes are within 2.4°C of modern throughout the record. The results suggest that the summer temperature changes in south-east margin of the Qinghai–T…
Evidence of Holocene climatic change and human impact in northwestern Yunnan Province
Open AccessXiayun Xiao, Simon Haberle et al.ARTICLEThe Holocene2017Cited by: 4References: 7
High-resolution pollen and charcoal records from Chenghai Lake, northwestern Yunnan Province of China, are presented in this study. These records reveal changes in climate and human activity since 8220 cal. yr BP, and the drivers of climatic change are further discussed based on spectral analysis of Tsuga and evergreen oak pollen percentages. The pollen record indicated that the climate in the low altitude area was relatively warm and moderately …
Asian summer monsoon variability during the late glacial and Holocene inferred from the stable carbon isotope record of black carbon in the sediments of Muge Co, southeastern Tibetan Plateau, China
Open AccessWeiwei Sun, Enlou Zhang et al.ARTICLEThe Holocene2015Cited by: 1References: 14
A sediment core from an alpine lake (Muge Co) from the southeastern margin of the Tibetan Plateau was analyzed for sediment grain size distribution and the carbon isotopic composition of black carbon in order to reconstruct Asian summer monsoon variability over the last 12 ka. Five major climatic stages were identified: (1) From 12 to 10.5 cal. ka BP, a cold and dry climate prevailed, corresponding to the Younger Dryas in the North Atlantic; (2) …
Chironomid-inferred environmental change over the past 1400 years in the shallow, eutrophic Taibai Lake (south-east China)
Open AccessYanmin Cao, Enlou Zhang et al.ARTICLEThe Holocene2014Cited by: 1References: 2
A sediment core from Taibai Lake, a shallow and eutrophic lake (SE China), was analysed for chironomids to track environmental changes in the lake. Nutrient dynamics over the past 1400 years were traced based on subfossil records and a regional chironomid-inferred total phosphorus (CI-TP) transfer function. Between ad 600 and 1370, the coexistence of several macrophyte-related taxa such as Dicrotendipes, Paratanytarsus and Endochironomus reflecte…

Evidence of Holocene climatic change and human impact in northwestern Yunnan Province
Open AccessXiayun Xiao, Simon Haberle et al.ARTICLEThe Holocene2017Cited by: 4References: 7
High-resolution pollen and charcoal records from Chenghai Lake, northwestern Yunnan Province of China, are presented in this study. These records reveal changes in climate and human activity since 8220 cal. yr BP, and the drivers of climatic change are further discussed based on spectral analysis of Tsuga and evergreen oak pollen percentages. The pollen record indicated that the climate in the low altitude area was relatively warm and moderately …
Summer temperature variability inferred from subfossil chironomid assemblages from the south-east margin of the Qinghai–Tibetan Plateau for the last 5000 years
Open AccessJie Chang, Enlou Zhang et al.ARTICLEThe Holocene2017Cited by: 1References: 16
We present a quantitative mean July temperature record spanning the last c. 5000 years from an alpine lake in south-western China. The reconstruction is based on the application of an established chironomid-based inference model using 100 lakes from the region. The reconstructed summer temperature changes are within 2.4°C of modern throughout the record. The results suggest that the summer temperature changes in south-east margin of the Qinghai–T…
Asian summer monsoon variability during the late glacial and Holocene inferred from the stable carbon isotope record of black carbon in the sediments of Muge Co, southeastern Tibetan Plateau, China
Open AccessWeiwei Sun, Enlou Zhang et al.ARTICLEThe Holocene2015Cited by: 1References: 14
A sediment core from an alpine lake (Muge Co) from the southeastern margin of the Tibetan Plateau was analyzed for sediment grain size distribution and the carbon isotopic composition of black carbon in order to reconstruct Asian summer monsoon variability over the last 12 ka. Five major climatic stages were identified: (1) From 12 to 10.5 cal. ka BP, a cold and dry climate prevailed, corresponding to the Younger Dryas in the North Atlantic; (2) …
Chironomid-inferred environmental change over the past 1400 years in the shallow, eutrophic Taibai Lake (south-east China)
Open AccessYanmin Cao, Enlou Zhang et al.ARTICLEThe Holocene2014Cited by: 1References: 2
A sediment core from Taibai Lake, a shallow and eutrophic lake (SE China), was analysed for chironomids to track environmental changes in the lake. Nutrient dynamics over the past 1400 years were traced based on subfossil records and a regional chironomid-inferred total phosphorus (CI-TP) transfer function. Between ad 600 and 1370, the coexistence of several macrophyte-related taxa such as Dicrotendipes, Paratanytarsus and Endochironomus reflecte…